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    Thermal Inertia of Conductivity Cells: Observations with a Sea-Bird Cell

    Source: Journal of Atmospheric and Oceanic Technology:;1990:;volume( 007 ):;issue: 005::page 756
    Author:
    Lueck, Rolf G.
    ,
    Picklo, James J.
    DOI: 10.1175/1520-0426(1990)007<0756:TIOCCO>2.0.CO;2
    Publisher: American Meteorological Society
    Abstract: We have examined the magnitude and relaxation time of the thermal anomaly of the fluid flowing through the conductivity cell manufactured by Sea-Bird Electronics (SBE) that is induced by the heat stored in the wall of this cell using oceanic data collected in a thermohaline staircase. The relaxation is 9 to 10 s, about twice the value predicted by Lueck, while the initial magnitude of the conductivity error is 2.8%, about 35% smaller than predicted. The error in the measured conductivity is significant and long-lived and results in density errors detectable for 45 s after the sensor enters an isopycnal layer. An efficient numerical algorithm removes the anomaly from the measured conductivity signal and clears the resulting error from the computed salinity and density.
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      Thermal Inertia of Conductivity Cells: Observations with a Sea-Bird Cell

    URI
    https://yetl.yabesh.ir/yetl1/handle/yetl/4201400
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    contributor authorLueck, Rolf G.
    contributor authorPicklo, James J.
    date accessioned2017-06-09T16:05:30Z
    date available2017-06-09T16:05:30Z
    date copyright1990/10/01
    date issued1990
    identifier issn0739-0572
    identifier otherams-607.pdf
    identifier urihttp://onlinelibrary.yabesh.ir/handle/yetl/4201400
    description abstractWe have examined the magnitude and relaxation time of the thermal anomaly of the fluid flowing through the conductivity cell manufactured by Sea-Bird Electronics (SBE) that is induced by the heat stored in the wall of this cell using oceanic data collected in a thermohaline staircase. The relaxation is 9 to 10 s, about twice the value predicted by Lueck, while the initial magnitude of the conductivity error is 2.8%, about 35% smaller than predicted. The error in the measured conductivity is significant and long-lived and results in density errors detectable for 45 s after the sensor enters an isopycnal layer. An efficient numerical algorithm removes the anomaly from the measured conductivity signal and clears the resulting error from the computed salinity and density.
    publisherAmerican Meteorological Society
    titleThermal Inertia of Conductivity Cells: Observations with a Sea-Bird Cell
    typeJournal Paper
    journal volume7
    journal issue5
    journal titleJournal of Atmospheric and Oceanic Technology
    identifier doi10.1175/1520-0426(1990)007<0756:TIOCCO>2.0.CO;2
    journal fristpage756
    journal lastpage768
    treeJournal of Atmospheric and Oceanic Technology:;1990:;volume( 007 ):;issue: 005
    contenttypeFulltext
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    DSpace software copyright © 2002-2015  DuraSpace
    نرم افزار کتابخانه دیجیتال "دی اسپیس" فارسی شده توسط یابش برای کتابخانه های ایرانی | تماس با یابش
    yabeshDSpacePersian